GROUNDWATER. Groundwater The Hydrologic Cycle Groundwater.

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Presentation transcript:

GROUNDWATER

Groundwater The Hydrologic Cycle

Groundwater

Groundwater Phreatic zone Vadose zone porosity

Groundwater Phreatic zone

Groundwater Porosity vs. Permeability: Porosity – the amount of water a rock can hold Porosity – the amount of water a rock can hold Permeability – the amount of water that can move through a rock in a given amount of time Permeability – the amount of water that can move through a rock in a given amount of time Which is more important?

Groundwater What is an aquifer? a layer of rock from which water can be easily extracted A layer of rock through which water does not move readily is called an aquitard or aquiclude

Groundwater An unconfined aquifer

Groundwater A confined (artesian) system

Groundwater How fast does groundwater move? Between: 1 meter/day, and 1 meter/year On average, ~ 10 cm/day What are the consequences of this slow movement?

Groundwater Artificial recharge ponds, N. California

Groundwater How does groundwater erode? Solution channels in limestone, England Groundwater can only erode by dissolution, usually helped by carbonic acid. Limestones are particularly susceptible

Groundwater An area dominated by groundwater erosion is called karst topography

Groundwater Evolution of cave system

Groundwater Satellite image of a karst terrain

Groundwater Areceibo, Puerto Rico – SETI radio antenna

Groundwater Sinkholes

Groundwater Winter Park, FL

Groundwater

Groundwater Sinkhole swallows 2 cars, St. Louis, November 26, 2007

Groundwater Karst towers, China

Groundwater The Stone Forest, China

Groundwater Infilled sinkholes

Groundwater Red paleosols (Molas Fm) in Leadville Ls, Molas Lake

Groundwater How does groundwater transport its sediment? Only one way, in solution. This is what makes hard water, but dissolved load typically only in parts per million (ppm)

Groundwater How does groundwater deposit its sediment? By precipitation. This may occur within pore spaces, helping lithify sediments, or in open spaces as dripstone

Groundwater

Groundwater

Groundwater

Groundwater

Groundwater Gypsum stalactites, Lechuguilla, NM

Groundwater Calcite cement in sandstone

Groundwater SiO 2 carried by groundwater replaces trees

Groundwater Types of groundwater: meteoric meteoric connate connate magmatic magmatic Any of the above may also be hydrothermal water

Groundwater

Groundwater

Groundwater

Groundwater Issues with groundwater use: Pros: agricultural, industrial, & agricultural, industrial, & domestic water geothermal energy geothermal energy natural filtration natural filtration Cons: ground subsidence ground subsidence depletion depletion pollution pollution salt water encroachment salt water encroachment

Groundwater Groundwater use by state

Groundwater Geothermal test well, Nevada

Groundwater

Groundwater

Groundwater Subsidence due to groundwater extraction, Mexico City

Groundwater Subsidence due to groundwater extraction, San Joaquin Valley, CA

Groundwater Salt water encroachment